Is Africa The Second Largest Continent In The World – An animated color map showing different continents. Depending on the condition and model, some containers may be combined or separated.
It is a container for any of the many geographic regions. Containers are usually defined by convention rather than by any strict criteria. A continent can be a separate land or part of a larger land such as Asia or Europe. Because of this, the number of contents varies; As many as seven or four regions of the world are generally considered continents. Most Glycospeakers recognize seven regions of the continent. From largest to smallest, these regions are: Asia, Africa, North America, South America, Antarctica, Europe, Australia.
Is Africa The Second Largest Continent In The World
Various variations link some of these regions to smaller continents; An example of this is the joining of North America and South America to America, Asia and Europe to Eurasia and Africa, and Asia and Europe to Afro-Eurasia.
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To divide the world’s land into geographic regions, oceanic islands are often connected to neighboring land. In this diagram, most of the island nations and territories of the Pacific Ocean are combined with the continent of Australia to form the geographic region of Oceania.
In geology, a continent is defined as “a single land mass larger than the Earth’s surface, including continental and continental shelves.”
Geological continents correspond to the seven major regions of continental crust that lie on tectonic plates, but do not include small continental fragments such as Madagascar, commonly known as microcontinents. Continental crust is known to exist only on Earth.
The idea of continentality was recognized in the 20th century. He says that the modern continents were formed by the breakup of the supercontinent (Pangaea), which formed hundreds of millions of years ago.
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Continents, by term, refer to large, continuous, discrete land masses that are completely separated by water bodies.
In recent designs where five or more continents are recognized, at least one pair of continents is connected to the earth in some way. The “large” criterion leads to an arbitrary classification: with an area of 2,166,086 square kilometers (836,330 sq mi), Greenland is the world’s largest island, while Australia has an area of 7,617,930 square kilometers. . . kilometers (2,941,300 square kilometers), the continent is considered the smallest.
All major land features of one continuous World Ocean divided into several oceanic compartments by continents and various geographical features.
With the coasts of the land or continent and any boundaries of the land of the continent. In this section, the term continental Europe (sometimes called “mainland” in the UK) refers to mainland Europe, excluding islands such as Great Britain, Iceland, Ireland and Malta, while the term Australia is the mainland. Australia except New Zealand, Guinea, Tasmania and other nearby islands. Similarly, the continental United States refers to “the 49 states (including Alaska, excluding Hawaii) located on the northern continent and the District of Columbia.”
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In terms of geology or physical geography, a continent can be defined as a continuous land area including a shallow, contiguous area (the continental shelf).
From this point of view, the edge of the continental shelf is the true edge of the continent, because the coasts change due to changes in sea level.
In this plan, the islands of Great Britain and Ireland are part of Europe, while the islands of Australia and New Guinea together form the continent.
The concept of a continent as a cultural entity can include oceanic islands and continental fragments outside the continental shelf. Thus, Iceland is considered part of Europe, and Madagascar is part of Africa. Extrapolating this idea to extremes, some geographers have grouped the Australian mainland with other Pacific islands into a single “quasi-continent” called Oceania. It divides the land surface of the earth into continents or quasi-continents.
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The criterion that each container is a separate field is usually decided by historical convention and practical usage. Of the world’s seven known continents, only Antarctica and Australia are completely separated from other continents by an ocean. Several continents are defined as “more or less discrete masses” rather than as completely separate bodies.
Africa and Asia are connected by the Isthmus of Suez, and North America and South America by the Isthmus of Panama. In any case, these places are not separated by water (with the exception of the Suez and Panama Canals, which are narrow and short and man-made). Both isthmuses continue to the mainland.
The continents of North America and South America are treated separately in a separate model. But they can also be considered as one of the continents called America. This attitude was common in the United States before World War II and is common in some Asian models on six continents.
The model of one American continent operates in France, Greece, Hungary, Italy, Malta, Portugal, Spain and Latin American countries.
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If the continuous landmass of Eurasia is counted as two separate continents (Asia and Europe), the discrete landmass criterion is completely ignored. From a physical and geographical point of view, Europe and India are large peninsulas of the Eurasian land. However, Europe is considered a continent with a relatively large area of 10,180,000 square kilometers (3,930,000 sq mi), while India, covering less than half of this area, is considered a subcontinent. In geology and geography, the abandoned view of Eurasia as one continent leads to a six-continent view of the world. Some believe that the division of Eurasia into Asia and Europe is a remnant of Eurocracy: “Because of their physical, cultural and historical diversity, China and India can be compared not to separate parts of Europe, but to the continent of Europe […]” .
However, for historical and cultural reasons, the perspective of Europe as a separate continent persists in almost all genres.
If the continents are clearly defined to include the entire land mass, then Africa, Asia and Europe form one continent, which can be called Afro-Eurasia.
With the concentration of the American continent, this model gives four continents from Afro-Eurasia, America, Antarctica and Australia.
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During the Pleistocene Ice Age, when sea levels were low, large areas of the continental shelf opened up as land, forming land bridges between Tasmania and mainland Australia.
At that time, Australia and New Guinea were one continent called Sahul. Similarly, Afro-Eurasia and America were connected by the Bering Land Bridge. Other islands, such as Great Britain, are attached to their continents. At that time, there were only three separate continents in the world: Africa-Eurasia-America, Antarctica, Australia-New Guinea (Sahul).
In Glico-speaking countries, geographers refer to the geographic region that includes most of the island regions and regions of the Pacific Ocean and mainland Australia as Oceania.
In some non-English-speaking countries, such as China, Poland, Russia, Oceania, it is considered a real continent, since the equivalent of the word “continent” has a much wider meaning, which can be translated as “the great divide”. of the earth”. with islands “The great land with the greater part of the Earth” (inclined to the land), not (inclined to the country).
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For a more detailed list of populations of continental regions and subregions, see List of continents and continental regions by population.
The following table shows the areas given by Cyclopedia Britannica for each continent according to the seven-continent model, including Australasia with Melanesia, Micronesia, and Polynesia as parts of Oceania. According to the United Nations Statistics Division’s 2021 estimate, even the continent’s population is based on a UN geoscheme that includes all of Egypt (including the Isthmus of Suez and Sinai), part of Africa, and all of Azerbaijan. Cyprus, Georgia, Indonesia, Kazakhstan and Turkey as part of Asia (including East Thrace), all of Russia (including Siberia) as part of Europe, all of Panama and North America as part of North America (including Hawaii) as part of North America and all From Chile (including Easter Island) to South America.
The scope and meaning of the term continent includes the geological past in addition to the present continents. Supercontinents are known, especially in the geological record, as the clusters that make up most of the world’s cratons or continental cores.
These include Vaalbara, Courland, Columbia, Rodinia, Pannotia and Pangea. Over time, the supercontinents became the great first continents.
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Some parts of continents are recognized as subcontinents, especially large peninsulas separated from the mainland by geographical features. The most famous example is the Indian subcontinent.
Additional examples include the Arabian Peninsula, the Southern Cone of South America, and Alaska in North America.
In most of these cases, the corresponding “subcontinents” are on tectonic plates distinct from the rest of the continent, which is the geological basis of the terminology.
Greenland, generally considered the world’s largest island on the northern coast of the North American plate, is sometimes called a subcontinent.
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